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    A Numerical Investigation of Resonant Inertial Response of the Ocean to Wind Forcing 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 006:;page 873
    Author(s): Crawford, G. B.; Large, W. G.
    Publisher: American Meteorological Society
    Abstract: A one-dimensional model of upper-ocean vertical mixing is used to investigate the ocean's response to idealized atmospheric storms over short (1?2 day) timescales. Initial ocean conditions are based on observations from ...
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    Observations and Simulations of Upper-Ocean Response to Wind Events during the Ocean Storms Experiment 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 011:;page 2831
    Author(s): Large, W. G.; Crawford, G. B.
    Publisher: American Meteorological Society
    Abstract: The Ocean Storms dataset is used to compile observations of the oceanic response to midlatitude storms. Of particular interest are episodic mixed layer temperature cooling events whose characteristics are reviewed. The ...
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    Accounting for Surface Wave Distortion of the Marine Wind Profile in Low-Level Ocean Storms Wind Measurements 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 011:;page 2959
    Author(s): Large, W. G.; Morzel, J.; Crawford, G. B.
    Publisher: American Meteorological Society
    Abstract: Marine wind measurements at three heights (3.0,4.5, and 5.0 m) from both moored and drifting buoys during the Ocean Storms Experiment are described. These winds are compared with each other, with winds from ships, from ...
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    Resonant Wind-Driven Mixing in the Ocean Boundary Layer 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 008:;page 1866
    Author(s): Skyllingstad, Eric D.; Smyth, W. D.; Crawford, G. B.
    Publisher: American Meteorological Society
    Abstract: The role of resonant wind forcing in the ocean boundary layer was examined using an ocean large-eddy simulation (LES) model. The model simulates turbulent flow in a box, measuring ?100?300 m on a side, whose top coincides ...
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